The most incompressible metal osmium at static pressures above 750 gigapascals

L. Dubrovinsky (), N. Dubrovinskaia, E. Bykova, M. Bykov, V. Prakapenka, C. Prescher, K. Glazyrin, H.-P. Liermann, M. Hanfland, M. Ekholm, Q. Feng, L. V. Pourovskii, M. I. Katsnelson, J. M. Wills and I. A. Abrikosov ()
Additional contact information
L. Dubrovinsky: Bavarian Research Institute of Experimental Geochemistry and Geophysics, University of Bayreuth
N. Dubrovinskaia: Laboratory of Crystallography, University of Bayreuth
E. Bykova: Bavarian Research Institute of Experimental Geochemistry and Geophysics, University of Bayreuth
M. Bykov: Laboratory of Crystallography, University of Bayreuth
V. Prakapenka: Center for Advanced Radiation Sources, University of Chicago
C. Prescher: Center for Advanced Radiation Sources, University of Chicago
K. Glazyrin: Photon Sciences, Deutsches Elektronen-Synchrotron (DESY)
H.-P. Liermann: Photon Sciences, Deutsches Elektronen-Synchrotron (DESY)
M. Hanfland: European Synchrotron Radiation Facility
M. Ekholm: Swedish e-Science Research Centre (SeRC), Linköping University
Q. Feng: Swedish e-Science Research Centre (SeRC), Linköping University
L. V. Pourovskii: Swedish e-Science Research Centre (SeRC), Linköping University
M. I. Katsnelson: Radboud University, Institute for Molecules and Materials
J. M. Wills: Los Alamos National Laboratory
I. A. Abrikosov: Chemistry and Biology (IFM), Linköping University

Nature, 2015, vol. 525, issue 7568, 226-229

Abstract: Subtle anomalies in how the structure of metallic osmium evolves with pressure are detected using powder X-ray diffraction measurements at ultra-high static pressures; the anomaly at 440 gigapascals is attributed to an electronic transition caused by pressure-induced interactions between core electrons.

Date: 2015
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DOI: 10.1038/nature14681

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